![]() |
![]() |
TUGR HOME SHORT STORIES |
The purpose of this geologic study is to compare two
different, structural cross-section models to determine which model best fits the
designated field area. Both models will use the same thirteen wells chosen by F. P.
Schweers in his article published in 1959. Schweers cross-sectional model looked at
the subsurface according to his interpretation of the structural features seen, which was
to mold the cross-section into a rabbit-ear anticline model. Our best
fit model of the cross-section is a backthrust feature into the Ardmore Basin as a
result of inversion in the Arbuckle Mountains. In this research project we apply the line-length balance method to prepare balanced cross-sections of the structural features seen in both cross-sections in the Milroy Field. The Milroy Field is a small, Southern Oklahoma reservoir that runs from Southeastern Stephens County into Northwestern Carter County. The cross-section used in this project begins in Stephens County, Section 23-T2S-R4W, continues into Section 24-T2S-R4W, and ends in Carter County, Section 18-T2S-R3W.
Send Comments and Questions to: ©Copyright 2000 The University of
Tulsa Graduate Review, All Rights Reserved. |